Paxite is a rare copper arsenide mineral typically occurring as massive or granular aggregates in hydrothermal veins. It is most commonly found alongside other copper-arsenic minerals such as koutekite and domeykite. Identification is difficult without laboratory analysis like X-ray diffraction or electron microprobe study due to its resemblance to other silver-white metallic minerals.
Is this paxite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch paxite with a known reference. Paxite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic, tarnishing black.
- 4Match the color rangeCompare against the expected color range: black, steel gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive.
Often confused with
Paxite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside paxite
Minerals reported to co-occur with paxite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuAs₂
- Mohs hardness
- 3.5-4
- Density
- 5.4 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic, tarnishing black
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive
- Cleavage
- Perfect along {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal calcite veins cutting diopside hornfels lenses, in pyroxene gneisses and mica schists
Where rockhounds find paxite
Classic worldwide localities
- Mohawk, Keeweenaw Co., Michigan, USA
- Černý Důl mine, Krkonoše (Giant Mountains), Czech Republic (type locality)
- Mühltal, Niederbeerbach, Odenwald, Hesse, Germany
Field-hunting tip
Where it forms: In hydrothermal calcite veins cutting diopside hornfels lenses, in pyroxene gneisses and mica schists. If you start seeing novákite, koutekite, arsenic in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop.







